{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1362544420848695040.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2000gl012175"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000GL012175"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000GL012175"}},{"identifier":{"@type":"NAID","@value":"30013369317"}}],"dc:title":[{"@value":"The 1741 Oshima‐Oshima Eruption: Extent and volume of submarine debris avalanche"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Oshima‐Oshima is a small volcanic island southwest off Hokkaido in Japan Sea. The violent eruption on August 29, 1741 caused a sector collapse of the north flank. Very destructive tsunami with 2000 casualties was also documented, but the generation mechanism has been controversial; volume of subaerial sector collapse, about 0.4 km³, was considered too small to generate such a devastating tsunami. We compile and analyze recently‐obtained swath bathymetry data around the island. The volcano is more than 2.3 km high from ocean bottom with its base diameter of 18 km. The total slide volume, both subaerial and submarine, is estimated as 2.4 km³, nearly an order of magnitude larger than the subaerial part. To the north of island, hummocky terrain of debris deposits extends in an area of 69 km² with the total volume of 2.5 km³, a value similar to the total slide volume. It is one of the largest debris avalanches in historic time, and probably responsible to the tsunami generation.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382544420848695041","@type":"Researcher","foaf:name":[{"@value":"Kenji Satake"}]},{"@id":"https://cir.nii.ac.jp/crid/1382544420848695040","@type":"Researcher","foaf:name":[{"@value":"Yukihiro Kato"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00948276"},{"@type":"EISSN","@value":"19448007"}],"prism:publicationName":[{"@value":"Geophysical Research Letters"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2001-02","prism:volume":"28","prism:number":"3","prism:startingPage":"427","prism:endingPage":"430"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2000GL012175"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2000GL012175"}],"createdAt":"2004-02-05","modifiedAt":"2023-11-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360016870100529408","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Volcanic Lateral Collapse Processes in Mafic Arc Edifices: A Review of Their Driving Processes, Types and Consequences"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285706120449024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Estimating the Topography Before Volcanic Sector Collapses Using Tsunami Survey Data and Numerical Simulations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285708268938752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical Simulation of the Landslide and Tsunami Due to the 1741 Oshima‐Oshima Eruption in Hokkaido, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204229070464","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Catastrophic Sector Collapses of Quaternary Volcanoes as Significant Sediment Sources in Japan"},{"@language":"ja","@value":"土砂供給源としてみた日本の第四紀火山における巨大山体崩壊"},{"@language":"ja-Kana","@value":"ドシャ キョウキュウ ゲン ト シテ ミタ ニホン ノ ダイ4キ カザン ニ オケル キョダイサンタイ ホウカイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001205202735104","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geomorphologic features of large-scale submarine debris-avalanche along Japan coast-Comparison of Oshima-Oshima Volcano in Hokkaido and off Kaimon Volcano in southern Kyushu-"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237514496","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Subaqueous distribution and volume estimation of the debris-avalanche deposit from the 1640 eruption of Hokkaido-Komagatake volcano, southwest Hokkaido, Japan"},{"@value":"海域に流入した北海道駒ケ岳火山１６４０年岩屑なだれ堆積物の分布と体積推定"},{"@language":"ja-Kana","@value":"カイイキ ニ リュウニュウ シタ ホッカイドウ コマガタケ カザン 1640ネン ガンセツ ナダレ タイセキブツ ノ ブンプ ト タイセキ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206239266304","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami deposits recognized in Okushiri Island, southwestern Hokkaido, Japan"},{"@language":"ja","@value":"北海道南西部奥尻島で発見された津波堆積物"},{"@language":"ja-Kana","@value":"ホッカイドウ ナンセイブ オクシリトウ デ ハッケン サレタ ツナミ タイセキブツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217169792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Submarine slides and marine geohazards:"},{"@language":"ja","@value":"海底地すべりと災害"},{"@value":"海底地すべりと災害 : これまでの研究成果と現状の問題点"},{"@language":"ja-Kana","@value":"カイテイ ジスベリ ト サイガイ : コレマデ ノ ケンキュウ セイカ ト ゲンジョウ ノ モンダイテン"},{"@value":"Submarine slides and marine geohazards: the study results so far and current problems"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763063205376","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"地すべりによる津波の平面水槽を用いた水理模型実験"},{"@language":"en","@value":"HYDRAULIC EXPERIMENTS OF TSUNAMI GENERATION WITH PLANE WATER TANK DUE TO LANDSLIDE"},{"@language":"ja-Kana","@value":"ジスベリ ニ ヨル ツナミ ノ ヘイメン スイソウ オ モチイタ スイリ モケイ ジッケン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390296906985889408","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimating the Sources for 17th Century Tsunami by Using Tsunami Deposits Distributed from the Northern Hidaka Coast to Uchiura Bay, Hokkaido, Japan"},{"@language":"ja","@value":"北海道日高海岸北部から内浦湾周辺に分布する17世紀の津波堆積物を再現する津波波源の推定"},{"@language":"ja-Kana","@value":"ホッカイドウ ヒダカ カイガン ホクブ カラ ウチウラワン シュウヘン ニ ブンプ スル 17セイキ ノ ツナミ タイセキブツ オ サイゲン スル ツナミハ ゲン ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390298355906274176","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Korean Records of a Probable Tsunami in the Japan Sea in May 1415"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238088946816","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Case Study of Tsunami Evaluation Triggered by Submarine Landslide"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713076218240","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Distribution of Active Faults in Japan Sea and Future Issues"},{"@language":"ja","@value":"日本海における活断層の分布と今後の課題"},{"@language":"ja-Kana","@value":"ニホンカイ ニ オケル カツダンソウ ノ ブンプ ト コンゴ ノ カダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390846609817406720","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tsunami deposits from the 1640 Hokkaido Komagatake eruption, north Japan: constraints on inundation heights and numerical simulation of volcanic debris avalanche-derived tsunami"},{"@language":"ja","@value":"1640年北海道駒ヶ岳噴火による津波堆積物の分布と津波規模の推定"},{"@language":"ja-Kana","@value":"1640ネン ホッカイドウ コマガタケ フンカ ニ ヨル ツナミ タイセキブツ ノ ブンプ ト ツナミ キボ ノ スイテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/2051151842097198848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Marine tephra in the Japan Sea sediments as a tool for paleoceanography and paleoclimatology"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2000gl012175"},{"@type":"CIA","@value":"30013369317"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0031_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.2328/jnds.39.1_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.3389/feart.2021.639825_references_DOI_FtBPJtoePUTg3wdOlLPBvzSy0Ex"},{"@type":"CROSSREF","@value":"10.1007/s00024-017-1589-8_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.1029/2018jb016166_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.1186/s40645-015-0068-z_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.3313/jls.46.19_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2016.0042_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.5026/jgeography.119.568_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.2208/kaigan.74.i_145_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.4294/zisin.2017-21_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.4294/zisin.2022-10_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.20965/jdr.2023.p0835_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2019.0032_references_DOI_Vt8KLSusxXiooduvZZH44rXGo05"}]}